Revealing the Molecular Basis for the Stability of Organic Matter in Alkaline Soils

The Science

Using sophisticated instrumentation and techniques available at the Environmental Molecular Sciences Laboratory (EMSL) as part of its Biogeochemical Transformations and Isotope & Chemical Analysis Integrated Research platforms, scientists conducted experiments using methods including X-ray diffraction, 57Fe-Mössbauer spectroscopy, X-ray photoemission spectroscopy, nanoscale secondary ion mass spectroscopy, and transmission electron microscopy to examine the organic matter stabilization processes in alkaline soils. They found that most of the organic matter was bound within calcium aggregates, rather than adsorbing to iron or aluminum minerals, as would be expected in acidic environments.

The Impact

Understanding how soil organic matter stores carbon and nutrients and acts as a sink for atmospheric carbon dioxide is important to agriculture and the global climate. Until now, most research has focused on organic matter’s adsorption to mineral surfaces in acidic conditions. This study adds new insight into organic matter accumulation in alkaline soils and suggests a different, unexpected stabilization mechanism.

Summary

A research team, which included scientists from Pacific Northwest National Laboratory, Oregon State University, Sandia National Laboratories, and Iowa State University studied alkaline soil samples taken from eastern Washington State, conducting soil sorption experiments with two types of iron-binding compounds (pyoverdine and enterobactin) known as siderophores. They examined the minerology and distribution of carbon- and nitrogen-containing siderophores on individual fine particles within the soil. Results indicated that siderophores aggregated with calcium-rich organic matter coatings rather than with bare mineral surfaces. This discovery suggests an adsorption mechanism by which organics aggregate within alkaline soils via cation bridging. The mechanism results in greater sorption of the more water soluble siderophore onto soil particles. This finding may help scientists understand the composition of organic carbon and nutrients that accumulate in alkaline soils.

Principal Investigator

Rene Boiteau
Pacific Northwest National Laboratory
[email protected]

Program Manager

Paul Bayer
U.S. Department of Energy, Biological and Environmental Research (SC-33)
Environmental System Science
[email protected]

Funding

This work was supported by the Office of Biological and Environmental Research (BER), within the U.S. Department of Energy (DOE) Office of Science and was conducted at the Environmental Molecular Sciences Laboratory (EMSL), a DOE Office of Science user facility. The Linus Pauling Postdoctoral Fellowship at Pacific Northwest National Laboratory (PNNL) also supported the work through its Laboratory-Directed Research and Development Program funds.

References